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Computer Graphics Global Illumination: Photon Mapping , Participating Media Lecture 1 2 Taku Komura. last lecture . Monte-Carlo Ray Tracing Path Tracing Bidirectional Path Tracing Photon Mapping. Today. Methods to accelerate the accuracy of photon mapping - PowerPoint PPT Presentation
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Computer GraphicsGlobal Illumination:
Photon Mapping, Participating Media
Lecture 12Taku Komura
2
last lecture
Monte-Carlo Ray Tracing Path Tracing Bidirectional Path Tracing
Photon Mapping
3
Today
Methods to accelerate the accuracy of photon mapping
Rendering Participating Media
Accelerating the accuracy of photon mapping
Combine with ray tracing to visualize the specular light visible from the camera
Shoot more photons towards directions where more samples are needed Caustics photon map
Tracing photons only towards specular surfaces
A Practical Two-Pass Algorithm
Building photon maps by photon tracing Separate the photon paths into different
categories according to the reflectance Rendering
Combining the radiance of difference light paths
Light Transport Notation
L: Lightsource E: Eye S: Specular reflection D: Diffuse reflection (k)+ one or more k events (k)* zero or more of k events (k)? zero or one k event (k|k’) a k or k’ event
Photon Tracing
Create two photon maps Global photon map (the usual photon map)
All Photons with property L(S|D)*D are stored. Caustics photon map
Created by tracing photons that hit the specular surfaces Cast the photons only toward specular objects LS+D
Rendering
Separate the irradiance into four groups Direct illumination (by ray tracing or global
photon map) : LD Diffuse indirect illumination (by global photon
map) : LD(S|D)+D Specular reflection (by ray tracing) L(S|D)*S Caustics (by caustics photon map) LS+D
Caustics Photon Map
Caustics require high resolution Need to cast more photons towards
surfaces that generates caustics Projection Map
Projection map A map of the geometry seen from the light source
Made of many cells – which is on if there is a geometry in that direction, and off if not
For a point light, it is a spherical projection For directional light, a planar projection Use a bounding sphere to represent the objects
Direct + Indirect + Specular
Why is photon mapping efficient?
It is a stochastic approach that estimates the radiance from a few number of samples Kernel density estimation
Can actively distribute samples to important areas Caustics photon map
14
Today
Methods to accelerate the accuracy of photon mapping
Rendering Participating Media
Participating Media Dusty air, clouds, silky water Translucent materials such as marble,
skin, and plants Photon mapping is good in handling
participating media In participating media, the light is
scattered to different directions
Single / Multiple scattering
The brightness of a point
Is decided by Out scattering Absorption In scattering
),(
xL
'
)',(
xLi
),(
xL
Light out-scattering
• The change in radiance, L, in the direction ω, due to out scattering is given by
• The change in radiance due to absorption is
),()(),()(
xLxxL s
tcoefficien absorption: )(
tcoefficien scattering : )(
),()(),()(
x
x
xLxxL
a
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In-scattering
• The change due to inscattering
where the incident radiance, Li, is integrated over all directions
p is called the phase function describing the distribution of the scattered light
4
')',(),',()(),()(
dxLxpxxL is
'
)',(
xLi
Phase function Isotropic scattering
Scattered in any random direction
Henyey-Greenstein Phase Function Scattered in the direction more
towards the front Dust, stone, clouds
4
1)( p
2
12
2
)cos21(4
1)(
gg
gp
11 g
Phase function
Examples
Cornell Box scene – isotropic, homogeneous participating medium.
200,000 photons used with 65,000 in the volume map. Radiance
estimate used 100 photons.
Cornell Box scene – anisotropic, homogeneous participating medium.
200,000 photons used with 65,000 in the volume map. Radiance
estimate used 50 photons.
Ray marching and single scattering
),()(),',()',(),( xxLexxxpxLxL x
s
N
li
t
• Now we compute how the light will be accumulated along a ray
• This is called ray marching
where N is the number of light sources and Li is
the radiance from each light source
The last term is the light entering from behind, which is attenuated by proceeding Δx
Ray marching through a finite size medium (Single Scattering)
),()(),',()',(),(1 xxLexxxpxLxL n
xsl
N
llin
t
),2( ),,( ),,(1
xxLxxLxL nnn
• For multiple scattering, it is necessary to integrate all the in-scattered radiance at every segment
• Here S sample rays are used to estimate the in-scattered light
Multiple scattering
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xxLe
xxxpxLS
xxxpxLxL
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ss
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• Photon mapping can efficiently handle multiple scattering
• The photons interact with the media and are scattered / absorbed
• The average distance the photon proceeds after each interaction is
• Here S sample rays are used to estimate the in-scattered light
Photon mapping participating media
t coefficienon terminati:
1
ast
t
t
d
Photon Scattering
• The photon is either absorbed or scattered• The probability of scattering is
• Deciding what happens by Russian Roulette
• Once the photon interacts with the media, it is stored in a volume photon map
t
s
absorbed isPhoton
scattered isPhoton [0,1]Given
Volume Radiance Estimate
• Same as we did for surface radiance estimate, locate n nearest photons and estimate the radiance
31
34
),(),',(),()(
r
xxfxL p
n
ppo
Rendering Participating Media
• By ray tracing • If a ray enters a participating media, we use
ray marching to integrate the illumination.
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)(),',()',(),(
)(
31
1
xxLe
xr
xxf
xxxpxLxL
nxx
pn
pl
sl
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llln
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Single scattering term
multiple scattering term
Examples
single scattering multiple scattering
Subsurface Scattering• In computer graphics, reflections of non-metallic materials
are usually approximated by diffuse reflections. • Light leaving from the same location where it enters the
object• For translucent materials such as marble, skin and milk, this
is a bad approximation• The light leaves from different locations
Single scattering
Direct single scattering: Compute the distance the light has
traveled and attenuate according to the distance
Indirect Multiple scattering : Photon maps
Subsurface Scattering by Photon Mapping
• Photon tracing – as explained before• Rendering – Ray marching
BSSRDF
• Bidirectional Scattering Surface Reflectance Distribution Function (BSSRDF)
• Relates the differential reflected radiance dLr, at x in the direction ω, to the differential incident flux, dΦ, at x’ from direction ω’.
• We can capture/model the BSSRDF and use it for rendering
)','(
),()',',,(
xd
xdLxxS
i
r
Rendering using BSSRDF
(a) sampling a BRDF (b) sampling a BSSRDF Collect samples of incoming rays over an area
http://graphics.ucsd.edu/~henrik/animations/BSSRDF-SIGGRAPH-ET2001.avi
Rendering by BSSRDF
Human skin reflectance simulated by
BRDF BSSRDF
• Readings : Realistic Image Synthesis Using Photon Mapping by Henrik Wann Jensen, AK Peters Chapter 9, 10